Linking hydrological variations at local scales to regional climate teleconnection patterns

• Published in: Hydrological Processes
• Main Authors: Rasouli, Kabir, Scharold, Karis, Mahmood, Taufique H., Glenn, Nancy F., Marks, Danny
• Other Authors: National Science Foundation, Natural Sciences and Engineering Research Council of Canada
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2020
• Subjects: Antarctic; Pacific; Antarc*; North Atlantic; North Atlantic oscillation
• Online Access: http://dx.doi.org/10.1002/hyp.13982; https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.13982; https://onlinelibrary.wiley.com/doi/full-xml/10.1002/hyp.13982; https://onlinelibrary.wiley.com/doi/am-pdf/10.1002/hyp.13982

Abstract Climate patterns over preceding years affect seasonal water and moisture conditions. The linkage between regional climate and local hydrology is challenging due to scale differences, both spatially and temporally. In this study, variance, correlation, and singular spectrum analyses were conducted to identify multiple hydroclimatic phases during which climate teleconnection patterns were related to hydrology of a small headwater basin in Idaho, USA. Combined field observations and simulations from a physically based hydrological model were used for this purpose. Results showed statistically significant relations between climate teleconnection patterns and hydrological fluxes in the basin, and climate indices explained up to 58% of hydrological variations. Antarctic Oscillation (AAO), North Atlantic Oscillation (NAO), and Pacific North America (PNA) patterns affected mountain hydrology, in that order, by decreasing annual runoff and rain on snow (ROS) runoff by 43% and 26% during a positive phase of NAO and 25% and 9% during a positive phase of PNA. AAO showed a significant association with the rainfall‐to‐precipitation ratio and explained 49% of its interannual variation. The runoff response was affected by the phase of climate variability indices and the legacy of past atmospheric conditions. Specifically, a switch in the phase of the teleconnection patterns of NAO and PNA caused a transition from wet to dry conditions in the basin. Positive AAO showed no relation with peak snow water equivalent and ROS runoff in the same year, but AAO in the preceding year explained 24 and 25% ( p < 0.05) of their variations, suggesting that the past atmospheric patterns are equally important as the present conditions in affecting local hydrology. Areas sheltered from the wind and acted as a source for snow transport showed the lowest (40% below normal) ROS runoff generation, which was associated with positive NAO that explained 33% ( p < 0.01) of its variation. The findings of this research highlighted the ...